frequent volcanic activity
Lithospheric plates are outlined by faults.
Mid-ocean ridges and deep sea trenches (with their associated volcanos). Also in limited areas strike-slip fault systems (e.g. California), continental collision zones (e.g. India & Asia), etc.
Most earthquakes occur where the edges of Earth's plates are.
Most earthquakes occur near plate boundaries.
It is possible to have continental and oceanic crust on the same plate. The only to this exception is with the Pacific plate which exists independently.
Lithospheric plates are outlined by faults.
frequent volcanic activity
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Edges of tectonic plates
Mid-ocean ridges and deep sea trenches (with their associated volcanos). Also in limited areas strike-slip fault systems (e.g. California), continental collision zones (e.g. India & Asia), etc.
The lines of earthquake epicenters most effectively outline the edges of the lithosphere plates. The epicenter refers to the point on the earth's surface above the focus of an earthquake.
The most common way for mountains to form is when two lithospheric plates collide. This can cause volcanism and folding of rocks in the crust forming mountain belts.
Most earthquakes occur where the edges of Earth's plates are.
About 3 cent. a year About 3 cent. a year About 3 cent. a year About 3 cent. a year
Volcanoes are most likely to form at the edges of the tectonic plates.
The lithosphere includes the crust (oceanic and continental) and the uppermost part of the mantle. The lithospheric plates are thinnest at the ocean, varying from between a few kilometers to 100 kilometers in deep-ocean basins. The continental lithosphere, on the other hand, is generally about 100 to 250 kilometers thick. The most important feature of the lithosphere is its divisions into lithospheric plates. These plates move and collide, creating earthquakes, fault lines, etc.
because the crust is thinner and the techtonic plates meet.